P. Pauliš, Libor Hrůzek, J. Sejkora, Oldřich Janeček, Ondřej Pour, Bohuslav Bureš, Blanka Šreinová
{"title":"Zeofylit, tobermorit, fluorapofylit-(K) a doprovodná zeolitová mineralizace z Křížového vrchu u Cvikova \nv Lužických horách (Česká republika)","authors":"P. Pauliš, Libor Hrůzek, J. Sejkora, Oldřich Janeček, Ondřej Pour, Bohuslav Bureš, Blanka Šreinová","doi":"10.46861/bmp.31.065","DOIUrl":null,"url":null,"abstract":"Zeophyllite, tobermorite, kenotobermorite, fluorapophylite-(K) and associated zeolites were found in cavities of Cenozoic basaltic rocks of small abandoned quarry at western slope of the Křížový vrch hill (443 m a.s.l.), 1.5 km NE from Cvikov, 13 km NNE from Česká Lípa, Lužické hory Mountains, Czech Republic. Zeophyllite forms colorless spherical aggregates with pearly lustre usually 3 - 4 mm in size, aggregates with diameter up to 1 cm were observed only rarely. It is trigonal, space group R-3, with unit-cell parameters refined from PXRD: a 9.362(2), c 36.470(12) Å and V = 2768.3(1.2) Å3. Chemical analyses of zeophyllite correspond to the empirical formula (Ca12.84Na0.07)Σ12.91(Si9.83Al0.26)Σ10.09 O28(OH)1.43 F8.42· 6H2O. Tobermorite occurs as snow-white hemispherical to spherical aggregates up to 1 cm in size, it replaces earlier zeophyllite. It is monoclinic, space group Bm, with unit-cell parameters refined from PXRD: a 6.714(4), b 17.375(4), c 22.670(8) Å, γ 123.31(3)° and V 938.2(1.3) Å3. On the base of chemical analyses, tobermorite with empirical formula (Ca4.55Na0.03K0.02)Σ4.60(Si5.40Al0.60)Σ6.00O15.56(OH)1.44·5H2O is accompanied by more rare Ca-poor kenotobermorite with empirical formula (Ca3.99Na0.04)Σ4.03(Si5.60Al0.40)Σ6.00O14.62(OH)2.38·5H2O. Fluorapophyllite-(K) forms abundant prismatic crystals up to 0.5 - 2 cm in size. It is colorless to white with vitreous to greasy lustre. It is tetragonal, space group P4/mnc, with unit-cell parameters refined from PXRD: a 9.0157(13), c 15.7889(19) Å and V = 1283.4(3) Å3. Chemical analyses of fluorapophyllite-(K) correspond to the empirical formula (K0.81Na0.24)Σ1.05Ca4.06(Si7.25Al0.47)Σ8.00O20F1.05· 8H2O. Other zeolites, thomsonite-Ca, chabazite-Ca, phillipsite-Ca and -K, were found in association; their PXRD data, unit-cell parameters and chemical compositions are given in the paper.","PeriodicalId":53145,"journal":{"name":"Bulletin Mineralogie Petrologie","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin Mineralogie Petrologie","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.46861/bmp.31.065","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 0
Abstract
Zeophyllite, tobermorite, kenotobermorite, fluorapophylite-(K) and associated zeolites were found in cavities of Cenozoic basaltic rocks of small abandoned quarry at western slope of the Křížový vrch hill (443 m a.s.l.), 1.5 km NE from Cvikov, 13 km NNE from Česká Lípa, Lužické hory Mountains, Czech Republic. Zeophyllite forms colorless spherical aggregates with pearly lustre usually 3 - 4 mm in size, aggregates with diameter up to 1 cm were observed only rarely. It is trigonal, space group R-3, with unit-cell parameters refined from PXRD: a 9.362(2), c 36.470(12) Å and V = 2768.3(1.2) Å3. Chemical analyses of zeophyllite correspond to the empirical formula (Ca12.84Na0.07)Σ12.91(Si9.83Al0.26)Σ10.09 O28(OH)1.43 F8.42· 6H2O. Tobermorite occurs as snow-white hemispherical to spherical aggregates up to 1 cm in size, it replaces earlier zeophyllite. It is monoclinic, space group Bm, with unit-cell parameters refined from PXRD: a 6.714(4), b 17.375(4), c 22.670(8) Å, γ 123.31(3)° and V 938.2(1.3) Å3. On the base of chemical analyses, tobermorite with empirical formula (Ca4.55Na0.03K0.02)Σ4.60(Si5.40Al0.60)Σ6.00O15.56(OH)1.44·5H2O is accompanied by more rare Ca-poor kenotobermorite with empirical formula (Ca3.99Na0.04)Σ4.03(Si5.60Al0.40)Σ6.00O14.62(OH)2.38·5H2O. Fluorapophyllite-(K) forms abundant prismatic crystals up to 0.5 - 2 cm in size. It is colorless to white with vitreous to greasy lustre. It is tetragonal, space group P4/mnc, with unit-cell parameters refined from PXRD: a 9.0157(13), c 15.7889(19) Å and V = 1283.4(3) Å3. Chemical analyses of fluorapophyllite-(K) correspond to the empirical formula (K0.81Na0.24)Σ1.05Ca4.06(Si7.25Al0.47)Σ8.00O20F1.05· 8H2O. Other zeolites, thomsonite-Ca, chabazite-Ca, phillipsite-Ca and -K, were found in association; their PXRD data, unit-cell parameters and chemical compositions are given in the paper.
期刊介绍:
Bulletin Mineralogie Petrologie is a peer-reviewed journal focused especially on: mineralogy, crystal chemistry and study of crystal structures of minerals study of mineral associations and processes of their origin meteoritics, research of tectites economic geology (of ore deposits) and study of history of mining of ore deposits topographic mineralogy petrology of igneous, metamorphic and sedimentary rocks instrumental analytical methods at mineralogy and petrology mineralogy and petrology as tools for archeology and similar disciplines